The soil of the hills west and east of the banks in the Mures Couloir are mainly brown eumesobasic soils and brown illuvial argillaceous soils, which can be found in standard formats on the wide flat peaks and in various stages of erosion on the slopes, where they are frequently combined with regosols and even erodisols, often anthropically modified by means of earthwork and fertilisation.

The dolomitic part of K1 is characterized to be mudstone, mudstone to packstone, beige, moderately hard to hard, crystalline to cryptocrystalline, have occasional pelloids, pebbles and shell fragments, have local mudcracks in mudstone, slightly argillaceous in parts, have thin layers of anhydrite and o have good to fair vuggy and intercrystalline porosity.

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